在室内人工模拟降雨条件下, 通过沿坡面垂直分段和分层结合布设不同的稀土元素, 研究坡面侵蚀的时空演变规律. 结果表明: 次降雨条件下在产流开始20 min内, 坡面片蚀和细沟侵蚀的平均侵蚀加速度、平均侵蚀率和累积侵蚀量之比分别为1:1, 1:1.5和1:1.3, 坡面下1/3区域的平均侵蚀加速度、平均侵蚀率和累积侵蚀量分别是坡面中部的5, 12, 13倍; 后期细沟平均侵蚀加速度、平均侵蚀率和累积侵蚀量分别为片蚀的43, 7, 5倍. 连续小雨强降雨条件下, 产流35 min内, 细沟侵蚀平均加速度是片蚀的7~10倍, 35 min后, 坡面处于稳定状态; 降雨产流10 min内, 坡面下1/3区域平均侵蚀加速度是坡面中部的5倍, 沟头激活后, 坡面中部的平均侵蚀加速度达到坡面下1/3区域的4倍; 坡顶部存在一个相对稳定区. 说明REE示踪技术能够同时量化随时间和空间变化的坡面侵蚀过程.
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